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Earthquake · Sunday, October 18, 2026

Magnitude 4.3 earthquake 67 km E of Petropavlovsk-Kamchatsky, Russia

A magnitude 4.3 (light) earthquake struck 67 km E of Petropavlovsk-Kamchatsky, Russia on Sunday, October 18, 2026 at , at a depth of 78 km (intermediate).

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Magnitude
4.3Light
Depth
78km · intermediate
Time
Epicenter
53.17° N
159.62° E
Aftershocks so far
4within 250 km
Largest aftershock
5.3M

22 days ago · USGS id us6000u347 · last revised

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The full globe opens the 3D cross-section: the hypocenter at depth, the plate boundary and subducting slab where there is one, the aftershock sequence as it grows, and the sea floor around an offshore epicenter.

What a magnitude 4.3 means

Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.

A magnitude 4.3 releases about 32 times the seismic energy of a magnitude 3.3, roughly the energy of 43 tonnes of TNT. Magnitude measures the energy released at the source; how hard the ground shook at any one place depends on distance, depth and local geology, and is reported separately as intensity.

Intermediate-depth earthquakes (70 to 300 km) occur inside subducting slabs. The extra distance to the surface spreads the shaking over a wider area at lower intensity.

Nearby earthquakes and aftershocks

This event is part of a sequence: a larger magnitude 6.9 struck 206 km away on Oct 16, 03:35 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.4 97 km 80 km 35 km SE of Vilyuchinsk, Russia
5.0 10 km 216 km 205 km SSE of Vilyuchinsk, Russia
5.3 70 km 116 km 101 km SSE of Vilyuchinsk, Russia
4.5 61 km 82 km 136 km NE of Petropavlovsk-Kamchatsky, Russia
before 6.9 135 km 206 km 76 km NE of Ozernovskiy, Russia
before 4.9 10 km 200 km 198 km SSE of Vilyuchinsk, Russia
before 4.5 183 km 132 km 82 km SSW of Mil’kovo, Russia
before 4.9 10 km 174 km 180 km SE of Vilyuchinsk, Russia
before 4.6 69 km 19 km 82 km E of Petropavlovsk-Kamchatsky, Russia
before 4.6 78 km 186 km 96 km NE of Ozernovskiy, Russia
before 4.8 10 km 160 km 191 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 34 km 111 km 138 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.4 84 km 15 km 58 km ENE of Petropavlovsk-Kamchatsky, Russia
before 4.8 10 km 242 km 194 km S of Ust’-Kamchatsk Staryy, Russia
before 5.1 10 km 181 km 182 km SSE of Vilyuchinsk, Russia
before 4.4 10 km 198 km 201 km SSE of Vilyuchinsk, Russia
before 4.2 10 km 157 km 189 km SE of Petropavlovsk-Kamchatsky, Russia
before 5.0 10 km 132 km 163 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 35 km 162 km 153 km SSE of Vilyuchinsk, Russia
before 4.4 93 km 145 km 52 km WSW of Paratunka, Russia
before 5.0 31 km 166 km 171 km SE of Vilyuchinsk, Russia
before 4.9 39 km 146 km 136 km SSE of Vilyuchinsk, Russia
before 5.0 10 km 178 km 179 km SSE of Vilyuchinsk, Russia
before 5.8 29 km 165 km 165 km SSE of Vilyuchinsk, Russia
before 4.9 32 km 100 km 136 km SE of Petropavlovsk-Kamchatsky, Russia
before 5.0 35 km 106 km 142 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.5 35 km 196 km 173 km SE of Atlasovo, Russia

Frequently asked questions

How is earthquake magnitude measured?

Modern magnitudes are moment magnitudes (Mw), computed from the seismic moment: the area of the fault that slipped, how far it slipped and the rigidity of the rock. Each whole step up the scale is about 32 times more energy, so a magnitude 7 releases roughly a thousand times the energy of a magnitude 5.

What is the difference between magnitude and intensity?

Magnitude is one number for the whole earthquake, describing the energy released at the source. Intensity describes the shaking at a particular place, on the Modified Mercalli scale from I (not felt) to X+ (extreme), and falls off with distance from the epicenter.

What is an aftershock?

An aftershock is a smaller earthquake in the same area after a larger one, as the crust around the ruptured fault adjusts to the new stresses. They are most frequent in the first hours and days and fade over weeks to months, though a large mainshock can produce aftershocks for years.

Why do the magnitude and location change?

The first solution uses the nearest stations only. As recordings arrive from more seismographs around the world, USGS revises the magnitude, depth and epicenter, sometimes several times in the first hours. This page reflects the latest revision.

Where does this earthquake data come from?

From the U.S. Geological Survey’s real-time earthquake feeds, which combine the USGS National Earthquake Information Center with regional seismic networks worldwide. EarthBrowser ingests the feed every minute.

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